Chemical reactions relevant to life may require reactants to become concentrated and organized rather than remaining highly diluted in a large body of water.
What natural environments could have concentrated useful prebiotic molecules and brought them together under conditions favorable for further chemistry?
Producing an organic molecule does not guarantee that it will participate in further useful reactions.
Molecules dispersed through an ocean or other large environment may be too dilute to react efficiently. Some mechanism of concentration, cycling, adsorption, confinement, or selective accumulation may therefore have been important.
Researchers study several natural concentration mechanisms. These include evaporation, wet-dry cycles, freezing, mineral surfaces, porous rocks, thermal gradients, phase separation, and small compartments.
Different environments can concentrate different molecules and can also change reaction rates and chemical stability.
The origin of life requires more than the production of ingredients. Those ingredients must encounter one another in useful combinations and under conditions where constructive reactions can compete with degradation and unwanted side reactions.
Laboratory studies show that environmental processes can concentrate organic molecules and influence their reactions.
Mineral surfaces, drying environments, pores, droplets, and other forms of confinement can alter local concentrations substantially.
Several origin-of-life models propose repeated environmental cycles in which molecules are produced, concentrated, reacted, dispersed, and concentrated again.
It remains uncertain which concentration mechanisms operated in the actual environment where life originated.
A process helpful for one chemical step may interfere with another, making compatibility among successive steps an important issue.
Proposed concentration mechanisms include evaporation, freezing, mineral adsorption, thermal gradients, porous environments, and phase separation.
The ability of ordinary physical processes to concentrate molecules should be included in any fair investigation of chemical origins.
The design question arises at the larger level: whether such processes are sufficient to move from heterogeneous chemistry toward the coordinated organization characteristic of even primitive life.
Natural concentration mechanisms are chemically plausible and experimentally demonstrable. Their role in the historical origin of life and their ability to support an entire sequence leading toward life remain subjects of research.